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| 1 | LARGE-SCALE STRIKE SLIP FAULT: THE MAJOR STRUCTURE OF INTRACONTINENTAL DEFORMATION AFTER COLLISION显示文摘Intracontinental deformation is one of the most interesting problems in tectonics. But so far little attention has been paid to rock deformation, metamorphism and magmatism related with large-scale displacement and rotation of these blocks. In this note, we take the Ailaoshan-Red River fault (ARF)zone in western Yunnan as an example and discuss the kinematics and dynamics of the fault With its neighbouring blocks in the Tertiary. | 钟大赉 P. TAPPONNIER 吴海威 张连生 嵇少丞 钟嘉猷 刘小汉 U. SCHAERER R. LACASSIU P. LELOUP | 1990 | Chinese Science Bulletin1990,35,4: | 23 |
| 2 | Ductile deformation within Upper Himalaya Crystalline Sequence and geological implications,in Nyalam area,Southern Tibet显示文摘The South Tibet Detachment System(STDS) is a flat normal fault that separates the Upper Himalaya Crystalline Sequence(UHCS) below from the Tethyan Sedimentary Sequence(TSS) above.Timing of deformations related to the STDS is critical to understand the mechanism and evolution of the Himalaya collision zone.The Nyalam detachment(ND)(~86°E) locates in the middle portion of STDS(81°-89°E).Dating of deformed leucocratic dykes that are most probably syntectonic at different depth beneath the ND,allow us to constrain the timing of deformation.(1) Dyke T11N37 located ~3500 m structurally below the ND emplaced at 27.4± 0.2 Ma;(2) Dyke T11N32 located ~1400 m structurally below the ND emplaced at 22.0±0.3 Ma;(3) T11N25 located within the top to the north STD shear zone,~150 m structurally below the ND,emplaced at 17.1±0.2 Ma.Combining ND footwall cooling history and T11N25 deformation temperature,we indicate a probable onset of top to the north deformation at ~16 Ma at this location.These results show an upward younging of the probable timing of onset of the deformation at different structural distance below the ND.We then propose a new model for deformation migration below the ND with deformation starting by pure shear deformation at depth prior to ~27.5 Ma that migrates upward at a rate of ~ 0.3 mm/a until ~18 Ma when deformation switches to top to the north shearing in the South Tibet Detachment shear zone(STDsz).As deformation on the ND stops at 14-13 Ma this would imply that significant top to the North motion would be limited to less than 5 Ma and would jeopardize the importance of lower channel flow. | LIU XiaoBing LIU XiaoHan LELOUP P.H. MAHEO G. PAQUETTE J.L. ZHANG XinGang ZHOU XueJun | 2012 | Chinese Science Bulletin2012,57,26: | 14 |
| 3 | Organic matter produced by algae and cyanobacteria: Quantitative and qualitative characterization显示文摘This work aims at characterizing organic matter produced by an alga Euglena gracilis and a cyanobacteria Microcystis aeruginosa and assessing the evolution of its characteristics during growth.A culture medium was optimized.The species growth phases were monitored using both visible spectrophotometry and flow cytometry cell counting.Organic matter fractionation according to hydrophobicity and specific UV absorbance(SUVA) index were used to specifically characterize the produced algal organic matter(AOM).The AOM characteristics were both growth phase and species dependent.However,a similar evolution was observed.The hydrophilic fraction(HPI) was the major fraction whatever the growth phases and was almost the only one produced during lag and exponential phases.It represented around 75% of AOM during exponential phase and then decreased when the stationary phase appeared.It represented 46% and 60% of the AOM during late decline phase for the cyanobacteria and the alga respectively.The hydrophobic(HPO) and transphilic(TPH) fractions started to appear from the beginning of the stationary phase with more hydrophobic compounds coming from intracellular organic material of dying cells.HPO and TPH percentages still increased during the decline phase probably because of two additional processes:photo-dissolution and leaching of particulate organic matter from cells fragments.A comparison of AOM during late decline phase and natural organic matter(NOM) from Glane River(France) underlined that AOM was more hydrophilic and presented a lower SUVA for each fractions than NOM.However,the difference between NOM and AOM hydrophobicity narrowed during decline phase. | Maud Leloup Rudy Nicolau Virginie Pallier Claude Yprmian Geneviève Feuillade-Cathalifaud | 2013 | Journal of Environmental Sciences2013,25,6: | 10 |
| 4 | 藏南聂拉木高喜马拉雅结晶岩系上部韧性变形年代学及地质意义显示文摘藏南拆离断层系(STDS)为低角度正断层,其上盘为特提斯喜马拉雅沉积岩系,下盘为高喜马拉雅结晶岩系.厘定与STDS有关的变形时限,对深入理解喜马拉雅造山带的变形机制与构造演化具重要意义.聂拉木拆离断层(ND)(86°E)位于STDS中段(81°~89°E),ND下盘不同构造位置(即采样点位与ND的构造距离)的变形花岗质岩脉具有一定程度的同构造特征,锆石-独居石U-Th/Pb年龄可以不同程度地厘定变形时间:(1)样品T11N37(ND下盘约3500m构造位置)的侵位年龄为27.4±0.2Ma;(2)样品T11N32(ND下盘约1400m构造位置)的侵位年龄为22.0±0.3Ma;(3)样品T11N25(ND下盘约150m构造位置)的侵位年龄为17.1±0.2Ma,结合ND下盘冷却历史和T11N25变形温度,认为其变形最晚开始时间约为16Ma.年代学结果表明,变形作用的最晚开始时间由下盘往拆离面逐渐变年轻.因此提出ND下盘变形迁移的新模式,即ND下盘在约27.5Ma之前开始纯剪切为主的变形作用,随后变形以约0.3mm/a的速率向拆离面移动,并于约18Ma在藏南拆离断层剪切带(STDsz)底部转化为简单剪切变形为主.由于ND变形结束于14~13Ma,这意味着北向剪切作用的持续时限小于约5Ma,对下地壳流动模型提出新的挑战. | 刘小兵 刘小汉 LELOUP P.H. MAHEO G. PAQUETTE J.L. 张鑫刚 周学君 | 2012 | 科学通报2012,57,17: | 6 |
| 5 | 老龄小鼠模型内皮细胞衰老导致射血分数保留的心力衰竭显示文摘由于全球老龄化,射血分数保留的心力衰竭(heart failure with preserved ejection fraction,HFpEF)发生率持续上升。虽然HFpEF的病理生理机制仍然不完全清楚,但通常认为内皮炎症发挥了核心作用。细胞衰老是一种与老化和炎症有关的细胞生长停滞过程。Gevaert等使用加速老化的小鼠(senescence-accelerated mice,SAM)模型探究细胞衰老在HFpEF发生发展中的作用。 | 刘莉 叶鹏 Gevaert AB Shakeri H Leloup AJ Van Hove CE De Meyer GRY Vrints CJ Lemmens K Van Craenenbroeck EM | 2017 | 中华高血压杂志2017,25,9: | 2 |
| 6 | Tectonic evolution of the Tancheng - Lujiang ( Tan - Lu ) fault via middle Triassic toEarly Cenozoic Paleomagnetic Data 显示文摘 | Gilder S A Leloup P H Courtillot V | 1999 | Journal of Geophysics Research1999,104,15: | 1 |
| 7 | Interactions be-tween a natural food web,shellfish farming and exoticspecies:The case of the Bay of Mont Saint Miche(l France)显示文摘 | Leloup F A Desroy N Mao P L | 2008 | Estuarine Coastal and Shelf Science2008,76,: | 1 |
| 8 | The Ailao Shah - Red River metamorphic belt: Tertiary left-lateral shear between Indochi- na and South China显示文摘 | Tapponnier P Lacassin R Leloup P H | 1990 | Nature1990,343,: | 1 |
| 9 | Physical properties and self-setting mechanism of calcium phosphate cements from calcium bio-dihydrogenophosphate monohydrate and calcium oxide显示文摘 | Serraj S Leloup J M | 1999 | J Mater Sci Mater Med1999,10,2: | 1 |
| 10 | Antibac- terial activity of glass- ionomer cements, compomers and resin composites: Relationship between acidity and material setting phase显示文摘 | Vermeersch G Leloup G Delmee M & Vreven J | 2005 | J OralRehabi2005,32,5: | 1 |
| 11 | High-temperature metamorphism in a major strike-slip shear zone: The Ailao Shan- Red Riv- er, People's Republic of China显示文摘 | Leloup P H Kienast J R | 1993 | Earth and Planetary Sci ence Letters1993,118,: | 1 |
| 12 | Pricing with local interations on agent-based electronic marketplaces显示文摘 | Leloup B | 2003 | Electronic Commerce Research and Applications2003,,2: | 1 |
| 13 | The autonomic nervous sys tern,adipose tissue plasticity, and energy baJance显示文摘 | Penicaucl L Cousin B Leloup C | 2000 | Nutrition2000,16,10: | 1 |
| 14 | α-Amylase adsorption on starch crystallites显示文摘 | Leloup V M Colonna P Ring S G | 2004 | Biotech Bioeng2004,38,: | 1 |
| 15 | Balancing mito- chondrial redox signaling: a key point in metabolic regu- lation显示文摘 | Leloup C Casteilla L Carriere A | 2011 | Antioxidants & redox signaling2011,14,3: | 1 |
| 16 | Influence of curing protocol on selected properties of light-curing polymers: Degree of conversion, volume contraction, elastic modulus, and glass transition temperature显示文摘 | Magali Dewaele Erik Asmussen Anne Peutzfeldt E. Christian Munksgaard Ana R. Benetti Gauthier Finné Ga?tane Leloup Jacques Devaux | 2009 | Dental Materials2009,,12: | 1 |
| 17 | New constraints on the structure, thermoehronology and timing of the Ailao Shan Red River shear zone, SE Asia显示文摘 | Leloup P H Amaud N Lacassin R | 2001 | Journal of Geophysical Research2001,66,: | 1 |
| 18 | Pricing with local interactions on Agent-based electronic marketplaces显示文摘 | LELOUP B | 2003 | Electronic Commerce Research and Applications2003,2,2: | 1 |
| 19 | The Ailao Shan/Red River metamorphic belt:tertiary leftlateral shear between Indochina and South China显示文摘 | Tappoinner P Lacassin R Leloup P H | 1990 | Nature1990,343,: | 1 |
| 20 | The Ailao Shan-Red River metamorphic belt: Tertiary left-lateral shear between lndochina and South China显示文摘 | Tappormier P Lacassin R Leloup P H | 1990 | Nature1990,343,: | 1 |